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American College of
Preventative Medicine
February 23, 2008
Austin, TX
Robert S. Webb
NOAA ESRL Climate Analysis Branch
formerly the Climate Diagnostics Center (CDC)
Boulder, Colorado
An Introduction to
Global Climate Change
Overview
• Global Climate Change:
Trends & Projections
• North America:
Trends & Projections
• Parting Thoughts
What is Climate
Climate is the aggregated pattern of weather,
meaning averages, extremes, timing, spatial
distribution of…
• hot & cold
• cloudy & clear
• humid & dry
• drizzles & downpours
• snowfall, snowpack, & snowmelt
• blizzards, tornadoes, & typhoons
Climate change means altered patterns.
Global average temperature is just one measure of the
state of the global climate as expressed in these patterns.
Small temperature changes  big changes in the patterns.
(after Holdren NCES, 2008)
What is an extreme event
(CCSP SAP 3.3)
Global Temperatures are increasing
Green bars show 95%
confidence intervals
the 15 hottest years all occurred since 1990
http://data.giss.nasa.gov/gistemp/graphs/
Warmest
9th Warmest
2007 Surface Temperature
Historic record of global climate change
Warming of the climate
system is unequivocal,
as is now evident from
observations of increases
in global average air and
ocean temperatures,
widespread melting of
snow and ice, and rising
global mean sea level.
Warm nights increasing
Cold nights decreasing
Frequency of occurrence of cold or warm temperatures for 202
global stations for 3 time periods:1901 to 1950 (black), 1951 to
1978 (blue) and 1979 to 2003 (red).
Proportion of extreme precipitation events
increasing in most areas
NH Winter NH Summer
The frequency of heavy precipitation events has increased over most
land areas - consistent with warming and increases of atmospheric
water vapor while more intense and longer droughts have been
observed since the 1970s, particularly in the tropics and subtropics.
Greenhouse gas concentrations
Compared to natural
changes over the past
10,000 years, the spike in
concentrations of CO2 &
CH4 in the past 250 years is
extraordinary.
Humans are responsible for
the recent dramatic
increase emissions. Fossil
CO2 & CH4 lack carbon-14,
and the observed drop in
atmospheric C-14 is
measurable.
(IPCC AR4 WG1, 2007)
Best estimate of global radiative forcing
Ranges of projected surface warming
multi-model averages for different emission
scenarios and assessed ranges of warming
(IPCC AR4, 2007)
Projected surface temperature changes
for the early and late 21st century
relative to the period 1980–1999
Continents Warm 50% more than oceans
Observed & simulated continental & global
scale changes in surface temperature
observed change
(black line);
climate models
simulations using
natural (blue) and
anthropogenic
(red) forcings
Projected percent changes in precipitation
for the period 2090–2099
(relative to 1980–1999)
Warmer climate  More Water Vapor in the atmosphere
but an expanded belt of subtropical aridity
NH Winter NH Summer
Changes in
the physical
and biological
systems and
surface
temperature
1970-2004
(IPCC WG2, 2007)
Observed trends in some biophysical and
socio-economic indicators in North America
(IPCC WG1, 2007)
Changes in the
percent of days in
a year above
three thresholds
for North America
for daily high (top)
and low (bottom)
temperature
CCSP SAP 3.3
U.S. national average “heat wave” index
defined as warm spells of 4 days in duration with mean
temperature exceeding the threshold for a 1 in 10 year event
CCSP SAP 3.3
Area of the U.S. with much above normal
daily high and low summer temperatures
CCSP SAP 3.3
Regions in where heavy and very heavy
precipitation has increased
CCSP SAP 3.3
Observed & simulated changes in
regional surface temperature
IPCC WG1, 2007
Days in a year averaged over North America when
daily low temperature is in the top 10% of warm
nights for 1961-90
CCSP SAP 3.3
Number of frost days per year
averaged over North America
CCSP SAP 3.3
Growing season length
averaged over North America
CCSP SAP 3.3
Rainfall on days in the top 5% of heavy precipitation days for
the period 1961-1990 averaged over North America
CCSP SAP 3.3
Projected increase in occurrence of extremely
rare hot days (a 1 in-20 year event)
(from Wehner 2005)
Possible
impacts of
climate
change due
to projected
changes in
extreme
weather and
climate
events
(IPCC, 2007)
Emerging Challenges
Pythons could squeeze lower third of USA
Feb 21, 2008 By Elizabeth
Weise, As climate change
warms the nation, giant
Burmese pythons could
colonize one-third of the USA,
from San Francisco across
the Southwest, Texas and the
South and up north along the
Virginia coast, according to
U.S. Geological Survey maps
released Wednesday.The
pythons can be 20 feet long
and 250 pounds. They are
highly adaptable to new
environments.
Current Range Projected Range ca. 2100
Valuable Resources
IPCC Reports
www.ipcc.ch
CCSP Reports
www.climatescience.gov
Backup Slides
Summary of relative direction, magnitude and
certainty of health impacts to changes in climate
CCSP SAP 4.6
Temperature-mortality relative risk functions
for 11 U.S. cities, 1973–1994
(Curriero et al. 2002)
Projected increase in occurrence of extremely
high rainfall days (a 1 in-20 year event)
(from Wehner 2005)
Drinking waterborne disease outbreaks
and 90 percentile precipitation events
(Curriero et al. 2001)

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WebbACPM15gdhjggder59jgfhjfsfhhbvvgv.ppt

  • 1. American College of Preventative Medicine February 23, 2008 Austin, TX Robert S. Webb NOAA ESRL Climate Analysis Branch formerly the Climate Diagnostics Center (CDC) Boulder, Colorado An Introduction to Global Climate Change
  • 2. Overview • Global Climate Change: Trends & Projections • North America: Trends & Projections • Parting Thoughts
  • 3. What is Climate Climate is the aggregated pattern of weather, meaning averages, extremes, timing, spatial distribution of… • hot & cold • cloudy & clear • humid & dry • drizzles & downpours • snowfall, snowpack, & snowmelt • blizzards, tornadoes, & typhoons Climate change means altered patterns. Global average temperature is just one measure of the state of the global climate as expressed in these patterns. Small temperature changes  big changes in the patterns. (after Holdren NCES, 2008)
  • 4. What is an extreme event (CCSP SAP 3.3)
  • 5. Global Temperatures are increasing Green bars show 95% confidence intervals the 15 hottest years all occurred since 1990 http://data.giss.nasa.gov/gistemp/graphs/
  • 7. Historic record of global climate change Warming of the climate system is unequivocal, as is now evident from observations of increases in global average air and ocean temperatures, widespread melting of snow and ice, and rising global mean sea level.
  • 8. Warm nights increasing Cold nights decreasing Frequency of occurrence of cold or warm temperatures for 202 global stations for 3 time periods:1901 to 1950 (black), 1951 to 1978 (blue) and 1979 to 2003 (red).
  • 9. Proportion of extreme precipitation events increasing in most areas NH Winter NH Summer The frequency of heavy precipitation events has increased over most land areas - consistent with warming and increases of atmospheric water vapor while more intense and longer droughts have been observed since the 1970s, particularly in the tropics and subtropics.
  • 10. Greenhouse gas concentrations Compared to natural changes over the past 10,000 years, the spike in concentrations of CO2 & CH4 in the past 250 years is extraordinary. Humans are responsible for the recent dramatic increase emissions. Fossil CO2 & CH4 lack carbon-14, and the observed drop in atmospheric C-14 is measurable. (IPCC AR4 WG1, 2007)
  • 11. Best estimate of global radiative forcing
  • 12. Ranges of projected surface warming multi-model averages for different emission scenarios and assessed ranges of warming (IPCC AR4, 2007)
  • 13. Projected surface temperature changes for the early and late 21st century relative to the period 1980–1999 Continents Warm 50% more than oceans
  • 14. Observed & simulated continental & global scale changes in surface temperature observed change (black line); climate models simulations using natural (blue) and anthropogenic (red) forcings
  • 15. Projected percent changes in precipitation for the period 2090–2099 (relative to 1980–1999) Warmer climate  More Water Vapor in the atmosphere but an expanded belt of subtropical aridity NH Winter NH Summer
  • 16. Changes in the physical and biological systems and surface temperature 1970-2004 (IPCC WG2, 2007)
  • 17. Observed trends in some biophysical and socio-economic indicators in North America (IPCC WG1, 2007)
  • 18. Changes in the percent of days in a year above three thresholds for North America for daily high (top) and low (bottom) temperature CCSP SAP 3.3
  • 19. U.S. national average “heat wave” index defined as warm spells of 4 days in duration with mean temperature exceeding the threshold for a 1 in 10 year event CCSP SAP 3.3
  • 20. Area of the U.S. with much above normal daily high and low summer temperatures CCSP SAP 3.3
  • 21. Regions in where heavy and very heavy precipitation has increased CCSP SAP 3.3
  • 22. Observed & simulated changes in regional surface temperature IPCC WG1, 2007
  • 23. Days in a year averaged over North America when daily low temperature is in the top 10% of warm nights for 1961-90 CCSP SAP 3.3
  • 24. Number of frost days per year averaged over North America CCSP SAP 3.3
  • 25. Growing season length averaged over North America CCSP SAP 3.3
  • 26. Rainfall on days in the top 5% of heavy precipitation days for the period 1961-1990 averaged over North America CCSP SAP 3.3
  • 27. Projected increase in occurrence of extremely rare hot days (a 1 in-20 year event) (from Wehner 2005)
  • 28. Possible impacts of climate change due to projected changes in extreme weather and climate events (IPCC, 2007)
  • 29. Emerging Challenges Pythons could squeeze lower third of USA Feb 21, 2008 By Elizabeth Weise, As climate change warms the nation, giant Burmese pythons could colonize one-third of the USA, from San Francisco across the Southwest, Texas and the South and up north along the Virginia coast, according to U.S. Geological Survey maps released Wednesday.The pythons can be 20 feet long and 250 pounds. They are highly adaptable to new environments. Current Range Projected Range ca. 2100
  • 30. Valuable Resources IPCC Reports www.ipcc.ch CCSP Reports www.climatescience.gov
  • 32. Summary of relative direction, magnitude and certainty of health impacts to changes in climate CCSP SAP 4.6
  • 33. Temperature-mortality relative risk functions for 11 U.S. cities, 1973–1994 (Curriero et al. 2002)
  • 34. Projected increase in occurrence of extremely high rainfall days (a 1 in-20 year event) (from Wehner 2005)
  • 35. Drinking waterborne disease outbreaks and 90 percentile precipitation events (Curriero et al. 2001)